<?xml version='1.0' encoding='utf-8'?>
<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:creator>C. W. Holmes</dc:creator>
  <dc:date>1984</dc:date>
  <dc:description>Distribution of210Pb in sediments on the South Texas Continental Shelf is related to dynamics of the sedimentary transport processes. This radioisotope, whose concentration is time-dependent, defines three depocenters on the shelf. In addition, the variation of210Pb activity at the sediment/water interface delineates areas of terrigenous sedimentation from hemipelagic sedimentation. ?? 1985 Springer-Verlag New York Inc.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1007/BF02281706</dc:identifier>
  <dc:language>en</dc:language>
  <dc:title>Natural radioisotope210Pb as an indicator of origin of fine-grained sediment</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>